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Revealing the natural complexity of fluvial morphology through 2D hydrodynamic delineation of river landforms Wyrick J.R., Senter A.E., Pasternick G.B., (2013) Evan Norman - Geographic Information Analysis - 2.27.2 Shaded relief map of a streambed
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Page 1: Morphological Unit (1) (1)

Revealing the natural complexity of fluvial morphology through 2D hydrodynamic delineation of river landformsWyrick J.R., Senter A.E., Pasternick G.B., (2013)

Evan Norman - Geographic Information Analysis - 2.27.2015

Shaded relief map of a streambed

Page 2: Morphological Unit (1) (1)

What is a morphological unit (MU)?

“Topographic forms within the river corridor that represent distinct form-process applications.”

-Controlled by ecohydraulic variables-Near-census-In this study, applicable at lengths ~1-10 times W

Page 3: Morphological Unit (1) (1)

How are MUs delineated?

Hydraulics (water flow)

+

DEM and LiDAR data (Landforms)

=

MU

Page 4: Morphological Unit (1) (1)

Why are MUs calculated?

-Describes underlying landforms in a river with 2D modeling

-Habitat assessments

Page 5: Morphological Unit (1) (1)

-Subjectivity

-Changing flow conditions

-“Ideal” conditions

-Increasing MU types

-Overlap of zones

-Flow direction

Drawbacks

Page 6: Morphological Unit (1) (1)

Example MU delineation procedure for a lowland gravel-cobble river

-Spatial Analyst- Raster calculator

-Irregular shapes

-Precise

-Thresholds are adjusted by discharge in model

More about MU mapping..

Page 7: Morphological Unit (1) (1)

Example MU delineation procedure for an upland cobble-boulder river

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Conclusions:

How do riffle-pool sequences correlate with discharge?

How are MUs distributed?

Lateral or longitudinal variability?

Spatial scales.

Riparian species.